| Reference Type | Journal (article/letter/editorial) |
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| Title | V.—On the Occurrence of Lead, Zinc, and Iron Ores, in some Rocks of Carboniferous Age in the North-West of England |
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| Journal | Geological Magazine |
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| Year | 1873 (February) | Series:Volume | 1:10 |
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| Issue | 104 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800470202 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 278328 | Long-form Identifier | mindat:1:5:278328:8 |
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| GUID | 0 |
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| Full Reference | (1873) V.—On the Occurrence of Lead, Zinc, and Iron Ores, in some Rocks of Carboniferous Age in the North-West of England. Geological Magazine, S. 1 Vol. 10 (104) 64-74 doi:10.1017/s0016756800470202 |
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| Plain Text | (1873) V.—On the Occurrence of Lead, Zinc, and Iron Ores, in some Rocks of Carboniferous Age in the North-West of England. Geological Magazine, S. 1 Vol. 10 (104) 64-74 doi:10.1017/s0016756800470202 |
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| In | (1873, February) Geological Magazine S. 1 Vol. 10 (104) Cambridge University Press (CUP) |
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| Abstract/Notes | In former papers I have described central Lancashire as capable of division into three plains of different elevations. The lowest being often beneath high-water mark, and always below the 25-foot Ordnance contour; the second ranging from 25 and 50 feet to 500 feet above the sea, terminating at the foot of the steep escarpment at the western edge of the Lancashire and Yorkshire moorlands forming the Pendle portion of the Pennine chain, with an average elevation of 1200 feet. Both the lower plains are much covered with drift, and the rock-surface at the sea-coast is often 50 feet below low-water mark, steadily rising in one gradual inclined plain, eastwards, or towards the Fells. |
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